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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/37RDSCE
Repositóriodpi.inpe.br/plutao@80/2010/07.11.14.14.18   (acesso restrito)
Última Atualização2010:08.12.13.14.01 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao@80/2010/07.11.14.14.19
Última Atualização dos Metadados2018:06.05.00.13.10 (UTC) administrator
Chave SecundáriaINPE--PRE/
ISSN0025-3227
Rótulolattes: 0307721738107549 2 CastroRossPess:2010:Fa&a&a
Chave de CitaçãoCastroRossPess:2010:Fa&#&#
TítuloFacies, δ13C, δ15N and C/N analyses in a late Quaternary compound estuarine fill, northern Brazil and relation to sea level
Ano2010
Data de Acesso13 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho3611 KiB
2. Contextualização
Autor1 Castro, Darciléa Ferreira
2 Rossetti, Dilce de Fátima
3 Pessenda, Luiz C. R.
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JGTQ
Grupo1
2 DSR-OBT-INPE-MCT-BR
Afiliação1 Universidade de São Paulo-USP, Instituto de Geociências – Programa de Geotectônica e Geoquímica
2 Rua do Lago, 562 Cidade Universitária 05508-080 São Paulo, SP, Brazil
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade de São Paulo, Laboratório de 14C, Av. Centenário 303, 13416000 Piracicaba, SP, Brazil
Endereço de e-Mail do Autor1
2 rossetti@dsr.inpe.br
Endereço de e-Mailrossetti@dsr.inpe.br
RevistaMarine Geology
Volume274
Páginas135-150
Histórico (UTC)2010-07-12 14:42:39 :: lattes -> marciana :: 2010
2010-08-12 13:14:01 :: marciana -> administrator :: 2010
2010-11-17 21:31:47 :: administrator -> marciana :: 2010
2011-05-26 23:58:49 :: marciana -> administrator :: 2010
2018-06-05 00:13:10 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chaveisótopos
Quaternário
paleoambiente
Ilha do Marajó
estuarine setting
sedimentary facies
isotopes
late Quaternary
relative sea-level
ResumoThe present work integrates sedimentary facies, 14C dating, δ13C, δ15N, and C/N with geologic and geomorphologic data available from literature. The aim was to characterize the depositional settings of a late Quaternary estuary in northeastern Marajó Island and analyze its evolution within the context of relative sea level fluctuations. The data derive from four continuous cores along a proximal-to-distal transect of a paleoestuary, previously recognized using remote sensing information. Fifteen sediment samples recorded ages ranging from 42,580 ± 1430 to 3184 ± 37 14C yr B.P. Facies analysis indicated fine- to coarse-grained sands with parallel lamination or cross stratification, massive or laminated muds and heterolithic deposits. δ13C (− 28.1 to − 19.7, mean = − 23.0), δ15N (+ 14.8 to + 4.7, mean = + 9.2) and C/N (14.5 to 1.5, mean = 7.9) indicate mostly marine and freshwater phytoplankton sources for the organic matter. The results confirm a large late Quaternary paleoestuary in northeastern Marajó Island. The distribution of δ13C, δ15N, and C/N, together with facies associations, led to identify depositional settings related to fluvial channel, floodplain, tidal channel/tidal flat, central basin, tidal delta, and tidal inlet/sand barrier. These deposits are consistent with a wave-dominated estuary. Variations in stratigraphy and geochemistry are controlled by changes in relative sea level, revealing a main transgression from an undetermined time around 42,000 14C yr B.P. and 29,340 (± 200) 14C yr B.P., which is synchronous to the overall drop in sea level after the last interglacial. Following this period, and probably until 9110 ± 37 14C yr B.P., i.e., during a time interval encompassing two glacial episodes including the Last Glacial and the Younger Dryas, there was a pronounced drop in sea level, recorded by the development of a major erosional discontinuity due to valley re-incision. Sea level rose again until 5464 ± 40 14C yr B.P, just before the main worldwide mid-Holocene transgressive peak. Mid to late Holocene coastal progradation ended the Marajó paleoestuarine history, and promoted the establishment of continental conditions throughout the island. The divergence comparing the Marajó sea level behavior with the eustatic curve allows hypothesizing that post-rifting tectonics along the Brazilian Equatorial margin influenced the sedimentary evolution of the studied paleoestuary. Considering that sedimentary facies in estuarine settings are highly variable both laterally and vertically, the present integration of facies with isotope and elemental analyses was crucial to provide a more precise interpretation of the Late Pleistocene and Holocene Marajó paleoestuary, and analyze its sea level history within the eustatic and tectonic context. .
ÁreaSRE
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Facies, {δ13C,} {δ15N}...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
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4. Condições de acesso e uso
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Arquivo Alvocastro.pdf
Grupo de Usuáriosadministrator
lattes
marciana
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
DivulgaçãoWEBSCI; PORTALCAPES.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
NotasSetores de Atividade: Outras atividades de serviços.
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel documentstage doi format isbn lineage mark mirrorrepository month nextedition number orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
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